| Dynamic Mechanism of Migmatization in the Dabie Complex, Northeastern Hubei, China |
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| 作者姓名： | Wang Jianghai Guangzhou Institute of New Geological Technology Academia Sini Guangzhou GuangdongYang Wenhua and Wu Jinping China U niversity of Geosciences W uhan Hubei Jiang M inxi |
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| 作者单位： | Wang Jianghai，Guangzhou Institute of New Geological Technology，Academia Sinica，Guangzhou，GuangdongYang Wenhua and Wu Jinping China U niversity of Geosciences，W uhan，Hubei Jiang M inxi |
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| 基金项目： | A project supported by the China National Natural Science Foundation(No.49070079) |
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| 摘 要： | On the basis of the detailed field work, compositions and contents of plagioclase and K - feldspar,determination of ordering degree, statistical analysis of plagioclase elongation index, mass-balance calculation and mineral spatial distribution and geochemistry, it is concluded that the migmatites in the Dabie complex are characterized by the presence of thermocenters. There are regular changes in mineral character in the migmatites from the centers outwards. The dominant genetic mechanism is anatexis and metasomatism, whose intensities decrease from the centers outwards. Finally, according to the simulated experiment on Liesegang' s rings and non-linear dynamics (dissipative structure theory), the dynamic mechanism of migmatization is profoundly expouded as consisting of the early-stage metasomatism induced by the thermal anomaly, the cardinal-stage anatexis induced by the early-stage matasomatism and finally the last-stage post-anatexis metasomatism.
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Dynamic Mechanism of Migmatization in the Dabie Complex, Northeastern Hubei, China |
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| Authors: | Wang Jianghai Guangzhou Institute of New Geological Technology Academia Sinic Guangzhou GuangdongYang Wenhua and Wu Jinping China U niversity of Geosciences W uhan Hubei Jiang M inxi |
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| Abstract: | On the basis of the detailed field work, compositions and contents of plagioclase and K - feldspar,determination of ordering degree, statistical analysis of plagioclase elongation index, mass-balance calculation and mineral spatial distribution and geochemistry, it is concluded that the migmatites in the Dabie complex are characterized by the presence of thermocenters. There are regular changes in mineral character in the migmatites from the centers outwards. The dominant genetic mechanism is anatexis and metasomatism, whose intensities decrease from the centers outwards. Finally, according to the simulated experiment on Liesegang' s rings and non-linear dynamics (dissipative structure theory), the dynamic mechanism of migmatization is profoundly expouded as consisting of the early-stage metasomatism induced by the thermal anomaly, the cardinal-stage anatexis induced by the early-stage matasomatism and finally the last-stage post-anatexis metasomatism. |
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| Keywords: | Dabie complex migmatites dynamic mechanism dissipative structure diffusion inverse to concentration gradients |
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